Dayuling Shan, Taiwan'da 3325 metre yüksekliğe sahiptir, Asia.
Bu zirve Fold Mountain olarak sınıflandırılır.
Yükselti
3325 m
Belirginlik
— m
Koordinatlar
24,183300, 121,283300
Tür
fold_mountain
On this page
Yükselti Karşılaştırması
Bu dağ hakkında
Dayuling Shan (3325m) is a fold mountain in Taiwan, Taiwan. Grade 3/5: strenuous climb with technical sections demanding experience. Formed by tectonic compression, it displays layered rock strata typical of fold ranges. Routes involve exposed ridge sections and require careful route-finding.
The topographic contour map of Dayuling Shan (3325m) shows elongated parallel contours following the ridge axis. Contour lines are drawn at 50m intervals, with index contours (thicker lines) every 250m. The hypsometric color scale ranges from green (lower elevations) through yellow and orange to white (highest elevations near the 3,325m summit).
Yükseklik profili
The east–west elevation profile of Dayuling Shan (3325m) shows the terrain cross-section through the summit at 3,325m. The color gradient transitions from green (valley floor) to white (summit zone), with the red summit marker indicating the peak.
Frequently Asked Questions
The contour map uses a hypsometric color scale where green represents lower elevations, yellow and orange indicate mid-range altitudes, and white marks the highest zones near the summit. Thicker contour lines (index contours) are drawn at wider intervals to help you quickly estimate elevation.
The contour map of Dayuling Shan (3325m) uses a 50m contour interval. This means each line represents a 50m change in elevation. Closely spaced contours indicate steeper terrain, while widely spaced contours show gentler slopes.
The elevation profile is a cross-section through Dayuling Shan (3325m) from west to east, passing through the summit at 3,325m. It reveals the mountain's shape, steepness, and relative height compared to the surrounding terrain. The horizontal axis shows distance in kilometers from the peak.
Dayuling Shan (3325m) was formed by tectonic folding, which compressed rock layers into long, parallel ridges. The contour map shows elongated lines that follow the axis of the fold, rather than circular patterns.
